Publication details

Emerald from the Anuri Prospect, Nunavut, Canada

Authors

GROAT Lee A. BRAND Allison CEMPÍREK Jan GRICE Joel WIGHT Willow

Year of publication 2019
Type Article in Periodical
Magazine / Source Journal of Gemmology
MU Faculty or unit

Faculty of Science

Citation
Web https://search.proquest.com/docview/2299784605/28E05AA8BE8045A1PQ/17?accountid=16531
Doi http://dx.doi.org/10.15506/JoG.2019.36.7.584
Keywords Emerald; gemstone; gemology; Canada
Description Ten polished thin sections of the seven intervals were studied with a petrographic microscope, scanning electron microscope and electron microprobe. The results show that the beryl occurs within a texturally and mineralogically variable matrix of phlogopite, muscovite, actinolite, plagioclase and pyrite, with occasional quartz, calcite and accessory minerals such as fluorapatite, titanite, rutile, chalcopyrite, molybdenite and rare tellurides. The beryl can occur as large, slightly altered grains in coarse-textured, hydrothermally altered, silicified zones, as well as at altered protolith contacts, as inclusions in other minerals (such as amphibole), and as a fine-grained, pervasive overprint that may represent a sodic alteration event.

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